【摘要】 基于强震动观测台钻孔数据,统计得到了四川、甘肃地区20m深的浅硬土层场地平均剪切波速模型.通过与美国加州地区的波速模型对比,结合四川、甘肃地区地震预报的地壳模型,延拓剪切波速模型至40km.应用四分之一波长法计算了浅硬土层场地的平均场地放大系数.利用场地放大系数,消除13次余震中浅硬场地的台站场地响应,反演了龙门山断层上、下盘的介质品质因子以及13次余震的有效应力降.通过与普通土层场地的强震动记录对比,对浅硬土层场地的放大系数进行调整,得到了深厚土层场地的平均放大系数.更多还原

【Abstract】 The average shear-wave velocity profile for shallow soil sites at a depth of 20 m is derived from the drilling data of strong motion stations in Sichuan and Gansu provinces.Combined with the profile of California and the crust model used in earthquake prediction study for Sichuan Province,the average shear-wave velocity profile is extended to 40 km.The site amplification factor for shallow soil sites is generated by using the quarter wave-length method.Then,the quality factors of different zones,the effective stress drop and kappa value at shallow soil sites are deduced from the Fourier amplitude spectra of 13 aftershocks of the Wenchuan earthquake.Due to different site effects,the strong motion data at deep soil sites show a large bias from the inverted model.According to the bias,the site amplification factor for deep soil sites is derived from revision of the site amplification factor for shallow soil sites.更多还原